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newmicro.F90 @ 5080

Last change on this file since 5080 was 2160, checked in by Laurent Fairhead, 10 years ago
Merged trunk changes -r2070:2158 into testing branch. Compilation problems introduced by revision r2155 have been corrected by hand
Property copyright set to Name of program: LMDZ Creation date: 1984 Version: LMDZ5 License: CeCILL version 2 Holder: Laboratoire de m\'et\'eorologie dynamique, CNRS, UMR 8539 See the license file in the root directory Property svn:eol-style set to `native` Property svn:keywords set to `Author Date Id Revision`
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1	! $Id: newmicro.F90 2160 2014-11-28 15:36:29Z abarral $
2
3
4
5	SUBROUTINE newmicro(ok_cdnc, bl95_b0, bl95_b1, paprs, pplay, t, pqlwp, pclc, &
6	pcltau, pclemi, pch, pcl, pcm, pct, pctlwp, xflwp, xfiwp, xflwc, xfiwc, &
7	mass_solu_aero, mass_solu_aero_pi, pcldtaupi, re, fl, reliq, reice, &
8	reliq_pi, reice_pi)
9
10	USE dimphy
11	USE phys_local_var_mod, ONLY: scdnc, cldncl, reffclwtop, lcc, reffclws, &
12	reffclwc, cldnvi, lcc3d, lcc3dcon, lcc3dstra
13	USE phys_state_var_mod, ONLY: rnebcon, clwcon
14	USE icefrac_lsc_mod ! computes ice fraction (JBM 3/14)
15	IMPLICIT NONE
16	! ======================================================================
17	! Auteur(s): Z.X. Li (LMD/CNRS) date: 19930910
18	! O. Boucher (LMD/CNRS) mise a jour en 201212
19	! Objet: Calculer epaisseur optique et emmissivite des nuages
20	! ======================================================================
21	! Arguments:
22	! ok_cdnc-input-L-flag pour calculer les rayons a partir des aerosols
23
24	! t-------input-R-temperature
25	! pqlwp---input-R-eau liquide nuageuse dans l'atmosphere dans la partie
26	! nuageuse (kg/kg)
27	! pclc----input-R-couverture nuageuse pour le rayonnement (0 a 1)
28	! mass_solu_aero-----input-R-total mass concentration for all soluble
29	! aerosols[ug/m^3]
30	! mass_solu_aero_pi--input-R-ditto, pre-industrial value
31
32	! bl95_b0-input-R-a PARAMETER, may be varied for tests (s-sea, l-land)
33	! bl95_b1-input-R-a PARAMETER, may be varied for tests ( -"- )
34
35	! re------output-R-Cloud droplet effective radius multiplied by fl [um]
36	! fl------output-R-Denominator to re, introduced to avoid problems in
37	! the averaging of the output. fl is the fraction of liquid
38	! water clouds within a grid cell
39
40	! pcltau--output-R-epaisseur optique des nuages
41	! pclemi--output-R-emissivite des nuages (0 a 1)
42	! pcldtaupi-output-R-pre-industrial value of cloud optical thickness,
43
44	! pcl-output-R-2D low-level cloud cover
45	! pcm-output-R-2D mid-level cloud cover
46	! pch-output-R-2D high-level cloud cover
47	! pct-output-R-2D total cloud cover
48	! ======================================================================
49
50	include "YOMCST.h"
51	include "nuage.h"
52	include "radepsi.h"
53	include "radopt.h"
54
55	! choix de l'hypothese de recouvrememnt nuageuse
56	LOGICAL random, maximum_random, maximum
57	PARAMETER (random=.FALSE., maximum_random=.TRUE., maximum=.FALSE.)
58
59	LOGICAL, SAVE :: first = .TRUE.
60	!$OMP THREADPRIVATE(FIRST)
61	INTEGER flag_max
62
63	! threshold PARAMETERs
64	REAL thres_tau, thres_neb
65	PARAMETER (thres_tau=0.3, thres_neb=0.001)
66
67	REAL phase3d(klon, klev)
68	REAL tcc(klon), ftmp(klon), lcc_integrat(klon), height(klon)
69
70	REAL paprs(klon, klev+1)
71	REAL pplay(klon, klev)
72	REAL t(klon, klev)
73	REAL pclc(klon, klev)
74	REAL pqlwp(klon, klev)
75	REAL pcltau(klon, klev)
76	REAL pclemi(klon, klev)
77	REAL pcldtaupi(klon, klev)
78
79	REAL pct(klon)
80	REAL pcl(klon)
81	REAL pcm(klon)
82	REAL pch(klon)
83	REAL pctlwp(klon)
84
85	LOGICAL lo
86
87	! !Abderr modif JL mail du 19.01.2011 18:31
88	! REAL cetahb, cetamb
89	! PARAMETER (cetahb = 0.45, cetamb = 0.80)
90	! Remplacer
91	! cetahb*paprs(i,1) par prmhc
92	! cetamb*paprs(i,1) par prlmc
93	REAL prmhc ! Pressure between medium and high level cloud in Pa
94	REAL prlmc ! Pressure between low and medium level cloud in Pa
95	PARAMETER (prmhc=440.100., prlmc=680.100.)
96
97	INTEGER i, k
98	REAL xflwp(klon), xfiwp(klon)
99	REAL xflwc(klon, klev), xfiwc(klon, klev)
100
101	REAL radius
102
103	REAL coef_froi, coef_chau
104	PARAMETER (coef_chau=0.13, coef_froi=0.09)
105
106	REAL seuil_neb
107	PARAMETER (seuil_neb=0.001)
108
109	! JBM (3/14) nexpo is replaced by exposant_glace
110	! INTEGER nexpo ! exponentiel pour glace/eau
111	! PARAMETER (nexpo=6)
112	! PARAMETER (nexpo=1)
113	! if iflag_t_glace=0, the old values are used:
114	REAL, PARAMETER :: t_glace_min_old = 258.
115	REAL, PARAMETER :: t_glace_max_old = 273.13
116
117	REAL rel, tc, rei
118	REAL k_ice0, k_ice, df
119	PARAMETER (k_ice0=0.005) ! units=m2/g
120	PARAMETER (df=1.66) ! diffusivity factor
121
122	! jq for the aerosol indirect effect
123	! jq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003
124	! jq
125	REAL mass_solu_aero(klon, klev) ! total mass concentration for all soluble aerosols [ug m-3]
126	REAL mass_solu_aero_pi(klon, klev) ! - " - (pre-industrial value)
127	REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3]
128	REAL re(klon, klev) ! cloud droplet effective radius [um]
129	REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value)
130	REAL re_pi(klon, klev) ! cloud droplet effective radius [um] (pi value)
131
132	REAL fl(klon, klev) ! xliq * rneb (denominator to re; fraction of liquid water clouds
133	! within the grid cell)
134
135	LOGICAL ok_cdnc
136	REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula
137
138	! jq-end
139	! IM cf. CR:parametres supplementaires
140	REAL zclear(klon)
141	REAL zcloud(klon)
142	REAL zcloudh(klon)
143	REAL zcloudm(klon)
144	REAL zcloudl(klon)
145	REAL rhodz(klon, klev) !--rho*dz pour la couche
146	REAL zrho(klon, klev) !--rho pour la couche
147	REAL dh(klon, klev) !--dz pour la couche
148	REAL zfice(klon, klev)
149	REAL rad_chaud(klon, klev) !--rayon pour les nuages chauds
150	REAL rad_chaud_pi(klon, klev) !--rayon pour les nuages chauds pre-industriels
151	REAL zflwp_var, zfiwp_var
152	REAL d_rei_dt
153
154	! Abderrahmane oct 2009
155	REAL reliq(klon, klev), reice(klon, klev)
156	REAL reliq_pi(klon, klev), reice_pi(klon, klev)
157
158	! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
159	! FH : 2011/05/24
160
161	! rei = ( rei_max - rei_min ) * T(°C) / 81.4 + rei_max
162	! to be used for a temperature in celcius T(°C) < 0
163	! rei=rei_min for T(°C) < -81.4
164
165	! Calcul de la pente de la relation entre rayon effective des cristaux
166	! et la température.
167	! Pour retrouver les résultats numériques de la version d'origine,
168	! on impose 0.71 quand on est proche de 0.71
169
170	d_rei_dt = (rei_max-rei_min)/81.4
171	IF (abs(d_rei_dt-0.71)<1.E-4) d_rei_dt = 0.71
172	! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
173
174	! Calculer l'epaisseur optique et l'emmissivite des nuages
175	! IM inversion des DO
176
177	xflwp = 0.D0
178	xfiwp = 0.D0
179	xflwc = 0.D0
180	xfiwc = 0.D0
181
182	reliq = 0.
183	reice = 0.
184	reliq_pi = 0.
185	reice_pi = 0.
186
187	IF (iflag_t_glace.EQ.0) THEN
188	DO k = 1, klev
189	DO i = 1, klon
190	! -layer calculation
191	rhodz(i, k) = (paprs(i,k)-paprs(i,k+1))/rg ! kg/m2
192	zrho(i, k) = pplay(i, k)/t(i, k)/rd ! kg/m3
193	dh(i, k) = rhodz(i, k)/zrho(i, k) ! m
194	! -Fraction of ice in cloud using a linear transition
195	zfice(i, k) = 1.0 - (t(i,k)-t_glace_min_old)/(t_glace_max_old-t_glace_min_old)
196	zfice(i, k) = min(max(zfice(i,k),0.0), 1.0)
197	! -IM Total Liquid/Ice water content
198	xflwc(i, k) = (1.-zfice(i,k))*pqlwp(i, k)
199	xfiwc(i, k) = zfice(i, k)*pqlwp(i, k)
200	END DO
201	END DO
202	ELSE ! of IF (iflag_t_glace.EQ.0)
203	DO k = 1, klev
204	CALL icefrac_lsc(klon,t(:,k),pplay(:,k)/paprs(:,1),zfice(:,k))
205
206
207	! JBM: icefrac_lsc is now contained icefrac_lsc_mod
208	! zfice(i, k) = icefrac_lsc(t(i,k), t_glace_min, &
209	! t_glace_max, exposant_glace)
210	DO i = 1, klon
211	! -layer calculation
212	rhodz(i, k) = (paprs(i,k)-paprs(i,k+1))/rg ! kg/m2
213	zrho(i, k) = pplay(i, k)/t(i, k)/rd ! kg/m3
214	dh(i, k) = rhodz(i, k)/zrho(i, k) ! m
215	! -IM Total Liquid/Ice water content
216	xflwc(i, k) = (1.-zfice(i,k))*pqlwp(i, k)
217	xfiwc(i, k) = zfice(i, k)*pqlwp(i, k)
218	END DO
219	END DO
220	ENDIF
221
222	IF (ok_cdnc) THEN
223
224	! --we compute cloud properties as a function of the aerosol load
225
226	DO k = 1, klev
227	DO i = 1, klon
228
229	! Formula "D" of Boucher and Lohmann, Tellus, 1995
230	! Cloud droplet number concentration (CDNC) is restricted
231	! to be within [20, 1000 cm^3]
232
233	! --present-day case
234	cdnc(i, k) = 10.*(bl95_b0+bl95_b1log(max(mass_solu_aero(i,k), &
235	1.E-4))/log(10.))*1.E6 !-m-3
236	cdnc(i, k) = min(1000.E6, max(20.E6,cdnc(i,k)))
237
238	! --pre-industrial case
239	cdnc_pi(i, k) = 10.*(bl95_b0+bl95_b1log(max(mass_solu_aero_pi(i,k), &
240	1.E-4))/log(10.))*1.E6 !-m-3
241	cdnc_pi(i, k) = min(1000.E6, max(20.E6,cdnc_pi(i,k)))
242
243	! --present-day case
244	rad_chaud(i, k) = 1.1((pqlwp(i,k)pplay(i, &
245	k)/(rdt(i,k)))/(4./3rpi1000.cdnc(i,k)))**(1./3.)
246	rad_chaud(i, k) = max(rad_chaud(i,k)*1.E6, 5.)
247
248	! --pre-industrial case
249	rad_chaud_pi(i, k) = 1.1((pqlwp(i,k)pplay(i, &
250	k)/(rdt(i,k)))/(4./3.rpi1000.cdnc_pi(i,k)))**(1./3.)
251	rad_chaud_pi(i, k) = max(rad_chaud_pi(i,k)*1.E6, 5.)
252
253	! --pre-industrial case
254	! --liquid/ice cloud water paths:
255	IF (pclc(i,k)<=seuil_neb) THEN
256
257	pcldtaupi(i, k) = 0.0
258
259	ELSE
260
261	zflwp_var = 1000.(1.-zfice(i,k))pqlwp(i, k)/pclc(i, k)* &
262	rhodz(i, k)
263	zfiwp_var = 1000.zfice(i, k)pqlwp(i, k)/pclc(i, k)*rhodz(i, k)
264	tc = t(i, k) - 273.15
265	rei = d_rei_dt*tc + rei_max
266	IF (tc<=-81.4) rei = rei_min
267
268	! -- cloud optical thickness :
269	! [for liquid clouds, traditional formula,
270	! for ice clouds, Ebert & Curry (1992)]
271
272	IF (zfiwp_var==0. .OR. rei<=0.) rei = 1.
273	pcldtaupi(i, k) = 3.0/2.0*zflwp_var/rad_chaud_pi(i, k) + &
274	zfiwp_var*(3.448E-03+2.431/rei)
275
276	END IF
277
278	END DO
279	END DO
280
281	ELSE !--not ok_cdnc
282
283	! -prescribed cloud droplet radius
284
285	DO k = 1, min(3, klev)
286	DO i = 1, klon
287	rad_chaud(i, k) = rad_chau2
288	rad_chaud_pi(i, k) = rad_chau2
289	END DO
290	END DO
291	DO k = min(3, klev) + 1, klev
292	DO i = 1, klon
293	rad_chaud(i, k) = rad_chau1
294	rad_chaud_pi(i, k) = rad_chau1
295	END DO
296	END DO
297
298	END IF !--ok_cdnc
299
300	! --computation of cloud optical depth and emissivity
301	! --in the general case
302
303	DO k = 1, klev
304	DO i = 1, klon
305
306	IF (pclc(i,k)<=seuil_neb) THEN
307
308	! effective cloud droplet radius (microns) for liquid water clouds:
309	! For output diagnostics cloud droplet effective radius [um]
310	! we multiply here with f * xl (fraction of liquid water
311	! clouds in the grid cell) to avoid problems in the averaging of the
312	! output.
313	! In the output of IOIPSL, derive the REAL cloud droplet
314	! effective radius as re/fl
315
316	fl(i, k) = seuil_neb*(1.-zfice(i,k))
317	re(i, k) = rad_chaud(i, k)*fl(i, k)
318	rel = 0.
319	rei = 0.
320	pclc(i, k) = 0.0
321	pcltau(i, k) = 0.0
322	pclemi(i, k) = 0.0
323
324	ELSE
325
326	! -- liquid/ice cloud water paths:
327
328	zflwp_var = 1000.(1.-zfice(i,k))pqlwp(i, k)/pclc(i, k)*rhodz(i, k)
329	zfiwp_var = 1000.zfice(i, k)pqlwp(i, k)/pclc(i, k)*rhodz(i, k)
330
331	! effective cloud droplet radius (microns) for liquid water clouds:
332	! For output diagnostics cloud droplet effective radius [um]
333	! we multiply here with f * xl (fraction of liquid water
334	! clouds in the grid cell) to avoid problems in the averaging of the
335	! output.
336	! In the output of IOIPSL, derive the REAL cloud droplet
337	! effective radius as re/fl
338
339	fl(i, k) = pclc(i, k)*(1.-zfice(i,k))
340	re(i, k) = rad_chaud(i, k)*fl(i, k)
341
342	rel = rad_chaud(i, k)
343
344	! for ice clouds: as a function of the ambiant temperature
345	! [formula used by Iacobellis and Somerville (2000), with an
346	! asymptotical value of 3.5 microns at T<-81.4 C added to be
347	! consistent with observations of Heymsfield et al. 1986]:
348	! 2011/05/24 : rei_min = 3.5 becomes a free PARAMETER as well as
349	! rei_max=61.29
350
351	tc = t(i, k) - 273.15
352	rei = d_rei_dt*tc + rei_max
353	IF (tc<=-81.4) rei = rei_min
354
355	! -- cloud optical thickness :
356	! [for liquid clouds, traditional formula,
357	! for ice clouds, Ebert & Curry (1992)]
358
359	IF (zflwp_var==0.) rel = 1.
360	IF (zfiwp_var==0. .OR. rei<=0.) rei = 1.
361	pcltau(i, k) = 3.0/2.0(zflwp_var/rel) + zfiwp_var(3.448E-03+2.431/ &
362	rei)
363
364	! -- cloud infrared emissivity:
365	! [the broadband infrared absorption coefficient is PARAMETERized
366	! as a function of the effective cld droplet radius]
367	! Ebert and Curry (1992) formula as used by Kiehl & Zender (1995):
368
369	k_ice = k_ice0 + 1.0/rei
370
371	pclemi(i, k) = 1.0 - exp(-coef_chauzflwp_var-dfk_ice*zfiwp_var)
372
373	END IF
374
375	reice(i, k) = rei
376
377	xflwp(i) = xflwp(i) + xflwc(i, k)*rhodz(i, k)
378	xfiwp(i) = xfiwp(i) + xfiwc(i, k)*rhodz(i, k)
379
380	END DO
381	END DO
382
383	! --if cloud droplet radius is fixed, then pcldtaupi=pcltau
384
385	IF (.NOT. ok_cdnc) THEN
386	DO k = 1, klev
387	DO i = 1, klon
388	pcldtaupi(i, k) = pcltau(i, k)
389	reice_pi(i, k) = reice(i, k)
390	END DO
391	END DO
392	END IF
393
394	DO k = 1, klev
395	DO i = 1, klon
396	reliq(i, k) = rad_chaud(i, k)
397	reliq_pi(i, k) = rad_chaud_pi(i, k)
398	reice_pi(i, k) = reice(i, k)
399	END DO
400	END DO
401
402	! COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS
403	! IM cf. CR:test: calcul prenant ou non en compte le recouvrement
404	! initialisations
405
406	DO i = 1, klon
407	zclear(i) = 1.
408	zcloud(i) = 0.
409	zcloudh(i) = 0.
410	zcloudm(i) = 0.
411	zcloudl(i) = 0.
412	pch(i) = 1.0
413	pcm(i) = 1.0
414	pcl(i) = 1.0
415	pctlwp(i) = 0.0
416	END DO
417
418	! --calculation of liquid water path
419
420	DO k = klev, 1, -1
421	DO i = 1, klon
422	pctlwp(i) = pctlwp(i) + pqlwp(i, k)*rhodz(i, k)
423	END DO
424	END DO
425
426	! --calculation of cloud properties with cloud overlap
427
428	IF (novlp==1) THEN
429	DO k = klev, 1, -1
430	DO i = 1, klon
431	zclear(i) = zclear(i)*(1.-max(pclc(i,k),zcloud(i)))/(1.-min(real( &
432	zcloud(i),kind=8),1.-zepsec))
433	pct(i) = 1. - zclear(i)
434	IF (paprs(i,k)<prmhc) THEN
435	pch(i) = pch(i)*(1.-max(pclc(i,k),zcloudh(i)))/(1.-min(real(zcloudh &
436	(i),kind=8),1.-zepsec))
437	zcloudh(i) = pclc(i, k)
438	ELSE IF (paprs(i,k)>=prmhc .AND. paprs(i,k)<prlmc) THEN
439	pcm(i) = pcm(i)*(1.-max(pclc(i,k),zcloudm(i)))/(1.-min(real(zcloudm &
440	(i),kind=8),1.-zepsec))
441	zcloudm(i) = pclc(i, k)
442	ELSE IF (paprs(i,k)>=prlmc) THEN
443	pcl(i) = pcl(i)*(1.-max(pclc(i,k),zcloudl(i)))/(1.-min(real(zcloudl &
444	(i),kind=8),1.-zepsec))
445	zcloudl(i) = pclc(i, k)
446	END IF
447	zcloud(i) = pclc(i, k)
448	END DO
449	END DO
450	ELSE IF (novlp==2) THEN
451	DO k = klev, 1, -1
452	DO i = 1, klon
453	zcloud(i) = max(pclc(i,k), zcloud(i))
454	pct(i) = zcloud(i)
455	IF (paprs(i,k)<prmhc) THEN
456	pch(i) = min(pclc(i,k), pch(i))
457	ELSE IF (paprs(i,k)>=prmhc .AND. paprs(i,k)<prlmc) THEN
458	pcm(i) = min(pclc(i,k), pcm(i))
459	ELSE IF (paprs(i,k)>=prlmc) THEN
460	pcl(i) = min(pclc(i,k), pcl(i))
461	END IF
462	END DO
463	END DO
464	ELSE IF (novlp==3) THEN
465	DO k = klev, 1, -1
466	DO i = 1, klon
467	zclear(i) = zclear(i)*(1.-pclc(i,k))
468	pct(i) = 1 - zclear(i)
469	IF (paprs(i,k)<prmhc) THEN
470	pch(i) = pch(i)*(1.0-pclc(i,k))
471	ELSE IF (paprs(i,k)>=prmhc .AND. paprs(i,k)<prlmc) THEN
472	pcm(i) = pcm(i)*(1.0-pclc(i,k))
473	ELSE IF (paprs(i,k)>=prlmc) THEN
474	pcl(i) = pcl(i)*(1.0-pclc(i,k))
475	END IF
476	END DO
477	END DO
478	END IF
479
480	DO i = 1, klon
481	pch(i) = 1. - pch(i)
482	pcm(i) = 1. - pcm(i)
483	pcl(i) = 1. - pcl(i)
484	END DO
485
486	! ========================================================
487	! DIAGNOSTICS CALCULATION FOR CMIP5 PROTOCOL
488	! ========================================================
489	! change by Nicolas Yan (LSCE)
490	! Cloud Droplet Number Concentration (CDNC) : 3D variable
491	! Fractionnal cover by liquid water cloud (LCC3D) : 3D variable
492	! Cloud Droplet Number Concentration at top of cloud (CLDNCL) : 2D variable
493	! Droplet effective radius at top of cloud (REFFCLWTOP) : 2D variable
494	! Fractionnal cover by liquid water at top of clouds (LCC) : 2D variable
495
496	IF (ok_cdnc) THEN
497
498	DO k = 1, klev
499	DO i = 1, klon
500	phase3d(i, k) = 1 - zfice(i, k)
501	IF (pclc(i,k)<=seuil_neb) THEN
502	lcc3d(i, k) = seuil_neb*phase3d(i, k)
503	ELSE
504	lcc3d(i, k) = pclc(i, k)*phase3d(i, k)
505	END IF
506	scdnc(i, k) = lcc3d(i, k)*cdnc(i, k) ! m-3
507	END DO
508	END DO
509
510	DO i = 1, klon
511	lcc(i) = 0.
512	reffclwtop(i) = 0.
513	cldncl(i) = 0.
514	IF (random .OR. maximum_random) tcc(i) = 1.
515	IF (maximum) tcc(i) = 0.
516	END DO
517
518	DO i = 1, klon
519	DO k = klev - 1, 1, -1 !From TOA down
520
521	! Test, if the cloud optical depth exceeds the necessary
522	! threshold:
523
524	IF (pcltau(i,k)>thres_tau .AND. pclc(i,k)>thres_neb) THEN
525
526	IF (maximum) THEN
527	IF (first) THEN
528	WRITE (, ) 'Hypothese de recouvrement: MAXIMUM'
529	first = .FALSE.
530	END IF
531	flag_max = -1.
532	ftmp(i) = max(tcc(i), pclc(i,k))
533	END IF
534
535	IF (random) THEN
536	IF (first) THEN
537	WRITE (, ) 'Hypothese de recouvrement: RANDOM'
538	first = .FALSE.
539	END IF
540	flag_max = 1.
541	ftmp(i) = tcc(i)*(1-pclc(i,k))
542	END IF
543
544	IF (maximum_random) THEN
545	IF (first) THEN
546	WRITE (, ) 'Hypothese de recouvrement: MAXIMUM_ &
547	& &
548	& RANDOM'
549	first = .FALSE.
550	END IF
551	flag_max = 1.
552	ftmp(i) = tcc(i)*(1.-max(pclc(i,k),pclc(i,k+1)))/(1.-min(pclc(i, &
553	k+1),1.-thres_neb))
554	END IF
555	! Effective radius of cloud droplet at top of cloud (m)
556	reffclwtop(i) = reffclwtop(i) + rad_chaud(i, k)1.0E-06phase3d(i, &
557	k)(tcc(i)-ftmp(i))flag_max
558	! CDNC at top of cloud (m-3)
559	cldncl(i) = cldncl(i) + cdnc(i, k)phase3d(i, k)(tcc(i)-ftmp(i))* &
560	flag_max
561	! Liquid Cloud Content at top of cloud
562	lcc(i) = lcc(i) + phase3d(i, k)(tcc(i)-ftmp(i))flag_max
563	! Total Cloud Content at top of cloud
564	tcc(i) = ftmp(i)
565
566	END IF ! is there a visible, not-too-small cloud?
567	END DO ! loop over k
568
569	IF (random .OR. maximum_random) tcc(i) = 1. - tcc(i)
570
571	END DO ! loop over i
572
573	! ! Convective and Stratiform Cloud Droplet Effective Radius (REFFCLWC
574	! REFFCLWS)
575	DO i = 1, klon
576	DO k = 1, klev
577	! Weight to be used for outputs: eau_liquide*couverture nuageuse
578	lcc3dcon(i, k) = rnebcon(i, k)phase3d(i, k)clwcon(i, k) ! eau liquide convective
579	lcc3dstra(i, k) = pclc(i, k)pqlwp(i, k)phase3d(i, k)
580	lcc3dstra(i, k) = lcc3dstra(i, k) - lcc3dcon(i, k) ! eau liquide stratiforme
581	lcc3dstra(i, k) = max(lcc3dstra(i,k), 0.0)
582	! Compute cloud droplet radius as above in meter
583	radius = 1.1((pqlwp(i,k)pplay(i,k)/(rdt(i,k)))/(4./3rpi1000. &
584	cdnc(i,k)))**(1./3.)
585	radius = max(radius, 5.E-6)
586	! Convective Cloud Droplet Effective Radius (REFFCLWC) : variable 3D
587	reffclwc(i, k) = radius
588	reffclwc(i, k) = reffclwc(i, k)*lcc3dcon(i, k)
589	! Stratiform Cloud Droplet Effective Radius (REFFCLWS) : variable 3D
590	reffclws(i, k) = radius
591	reffclws(i, k) = reffclws(i, k)*lcc3dstra(i, k)
592	END DO !klev
593	END DO !klon
594
595	! Column Integrated Cloud Droplet Number (CLDNVI) : variable 2D
596
597	DO i = 1, klon
598	cldnvi(i) = 0.
599	lcc_integrat(i) = 0.
600	height(i) = 0.
601	DO k = 1, klev
602	cldnvi(i) = cldnvi(i) + cdnc(i, k)lcc3d(i, k)dh(i, k)
603	lcc_integrat(i) = lcc_integrat(i) + lcc3d(i, k)*dh(i, k)
604	height(i) = height(i) + dh(i, k)
605	END DO ! klev
606	lcc_integrat(i) = lcc_integrat(i)/height(i)
607	IF (lcc_integrat(i)<=1.0E-03) THEN
608	cldnvi(i) = cldnvi(i)*lcc(i)/seuil_neb
609	ELSE
610	cldnvi(i) = cldnvi(i)*lcc(i)/lcc_integrat(i)
611	END IF
612	END DO ! klon
613
614	DO i = 1, klon
615	DO k = 1, klev
616	IF (scdnc(i,k)<=0.0) scdnc(i, k) = 0.0
617	IF (reffclws(i,k)<=0.0) reffclws(i, k) = 0.0
618	IF (reffclwc(i,k)<=0.0) reffclwc(i, k) = 0.0
619	IF (lcc3d(i,k)<=0.0) lcc3d(i, k) = 0.0
620	IF (lcc3dcon(i,k)<=0.0) lcc3dcon(i, k) = 0.0
621	IF (lcc3dstra(i,k)<=0.0) lcc3dstra(i, k) = 0.0
622	END DO
623	IF (reffclwtop(i)<=0.0) reffclwtop(i) = 0.0
624	IF (cldncl(i)<=0.0) cldncl(i) = 0.0
625	IF (cldnvi(i)<=0.0) cldnvi(i) = 0.0
626	IF (lcc(i)<=0.0) lcc(i) = 0.0
627	END DO
628
629	END IF !ok_cdnc
630
631	RETURN
632
633	END SUBROUTINE newmicro

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